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A travel time curve provides a graphical representation of the relationship between the travel time of seismic waves and their distance from the source of the seismic event. It helps in understanding how different types of seismic waves (such as P-waves and S-waves) propagate through various geological materials. By analyzing the curve, geologists and seismologists can infer subsurface structures and properties, aiding in the interpretation of seismic data for applications like earthquake analysis and oil exploration.

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